{"id":485,"date":"2023-08-17T19:14:50","date_gmt":"2023-08-17T11:14:50","guid":{"rendered":"https:\/\/hydro.as.ntu.edu.tw\/chia\/?page_id=485"},"modified":"2023-08-17T19:24:36","modified_gmt":"2023-08-17T11:24:36","slug":"2023-poster","status":"publish","type":"page","link":"https:\/\/hydro.as.ntu.edu.tw\/chia\/chia-forum-2023\/2023-poster\/","title":{"rendered":"CHiA Forum 2023 Poster"},"content":{"rendered":"\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t\t
\n\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t\t
\n\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t

Day 2-3<\/h2>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t

8\/22\u300123
Posters<\/span>
<\/h2>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t\t
\n\t\t\t\n\t\t\t\t\t\t<\/span>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t
\n\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t\t\t\t

\u5730\u9ede\uff1a\u4e2d\u7814\u9662\u4eba\u6587\u9928\u9928\u5317\u68df3\u6a13\u7b2c\u4e00\u6703\u8b70\u5ba4
\u6642\u9593\uff1a2023\/08\/21-2023\/08\/23<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t

\n\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t\t\t\t
\n\t\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\t\t\t\t8\/21 MON<\/span>\n\t\t\t\t\t<\/span>\n\t\t\t\t\t<\/a>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t\t\t\t
\n\t\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\t\t\t\t8\/22 TUE<\/span>\n\t\t\t\t\t<\/span>\n\t\t\t\t\t<\/a>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t\t\t\t
\n\t\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\t\t\t\t8\/23 WEN<\/span>\n\t\t\t\t\t<\/span>\n\t\t\t\t\t<\/a>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t\t
\n\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\n\t\t
\n\n\t\t\t\n\t\t\t\t
Poster Section I<\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
\n\n\t\t\t\t\t
Day 2 (8\/22) 16:00-17:30<\/div>\n\n\t\t\t\t\t\n\t\t\t\t<\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
\n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n
1<\/td>\n \u674e\u5b9c\u4ead <\/td>\n 2013-2022\u5e74\u677e\u5c71\u6a5f\u5834\u4f4e\u7a7a\u98a8\u5207\u4e4b\u7814\u7a76 <\/td>\n <\/tr>\n
2<\/td>\n \u6d2a\u7fca\u5f6c <\/td>\n On the Energetics of Convectively Coupled Kelvin Waves<\/td>\n <\/tr>\n
3<\/td>\n Dang Dong Pha<\/td>\n On the MJO diversity: A new GMS-plane analysis under the CQE framework<\/td>\n <\/tr>\n
4<\/td>\n Kai-Chih Tseng<\/td>\n The predictability of subtropical high and its implication for future projection<\/td>\n <\/tr>\n
5<\/td>\n Sieu-Cuong San (\u9673\u7d39\u5f37) <\/td>\n The Role of Off-equatorial Subsurface Temperature Anomalies to the Phase Reversal of Tropical Pacific Decadal Variability<\/td>\n <\/tr>\n
6<\/td>\n \u8607\u5bb9\u7469 <\/td>\n Analyzing the Mechanisms of Precipitation Change under Global Warming over the Tropical Ocean Using CMIP6 Data<\/td>\n <\/tr>\n
7<\/td>\n \u6c5f\u921e <\/td>\n Weakening of the linkage between the Southern China early spring rainfall and tropical heating(SST) since 2000<\/td>\n <\/tr>\n
8<\/td>\n \u674e\u739f\u828a <\/td>\n The critical role of highly oxygenated organic compounds for cloud droplet activation of biogenic organic aerosol particles<\/td>\n <\/tr>\n
9<\/td>\n \u738b\u9038 <\/td>\n The Impacts of Arctic Sea-ice Loss, Atlantic and Pacific Decadal Variability on the Sudden Stratospheric Warming Events.<\/td>\n <\/tr>\n
10<\/td>\n \u8b1d\u627f\u52f3 <\/td>\n CMIP6\u6a21\u5f0f\u5728\u5e74\u4ee3\u969b\u9810\u5831\u7684\u521d\u6b65\u8a55\u4f30 <\/td>\n <\/tr>\n
11<\/td>\n \u5468\u5f65\u5ef7 <\/td>\n The Effects of Natural Climate Variation and Anthropogenic Change on the Maritime Continent's Interannual Precipitation Variation.<\/td>\n <\/tr>\n
12<\/td>\n \u7f85\u6587\u65b0 <\/td>\n Southern Ocean SST response to a rapid Northern Hemisphere warming<\/td>\n <\/tr>\n
13<\/td>\n \u5433\u5f65\u797a <\/td>\n Wind Stress Variability Leads to Arctic Ocean Cooling via Ocean Heat Transports<\/td>\n <\/tr>\n
14<\/td>\n \u90b1\u6bd3\u5ead <\/td>\n Exploring the Impact of Climate Change on Amazon Hydroclimate Using the CESM2 Large Ensemble<\/td>\n <\/tr>\n
15<\/td>\n \u5f35\u5b87\u6cd3 <\/td>\n A Physical Storyline for the Response of Orographically-Locked Diurnal Convection in a Warming Scenario<\/td>\n <\/tr>\n
16<\/td>\n \u8096\u9db4\u9cf4 <\/td>\n The remote response in the Northern Pacific climate during winter to deforestation in the Maritime Continent<\/td>\n <\/tr>\n
17<\/td>\n \u90ed\u4f73\u6b23 <\/td>\n Exploring the Link between Multi-Scale Moisture Transport Patterns and Extreme Rainfall Events in the Asian-Australian Monsoon Region<\/td>\n <\/tr>\n
18<\/td>\n \u9ec3\u61f7\u9038 <\/td>\n Understanding the physical mechanisms of winter extreme precipitation over northern Taiwan<\/td>\n <\/tr>\n
19<\/td>\n \u674e\u5ead\u6167 <\/td>\n The role of maritime continent\u2019s rainforests in moderating the local interannual evapotranspiration variation<\/td>\n <\/tr>\n
20<\/td>\n \u674e\u601d\u7469 <\/td>\n \u6975\u7aef\u9ad8\u6eab\u76e3\u6e2c\u9810\u8b66\u7cfb\u7d71 <\/td>\n <\/tr>\n
21<\/td>\n \u6797\u6dd1\u8ed2 <\/td>\n Role of Diurnal Cycle in the Maritime Continent Barrier Effect on MJO Propagation in CMIP6<\/td>\n <\/tr>\n
22<\/td>\n Suranjith Bandara Koralegedara<\/td>\n Exploring Seasonal and Interannual Diurnal Rainfall Variations and the Underlying Mechanisms over a Tropical Island of Sri Lanka<\/td>\n <\/tr>\n
23<\/td>\n \u5468\u8a69\u502a <\/td>\n Stronger Arctic Amplification Produced by Decreasing, not increasing, CO2 Concentrations<\/td>\n <\/tr>\n
24<\/td>\n \u8a31 \u6840 <\/td>\n Forest Loss Could Trigger Tipping Point for Extreme Precipitation Events in Maritime Continent<\/td>\n <\/tr>\n
25<\/td>\n JIN-DE HUANG<\/td>\n The Role of Convection in Troposphere-Lower Stratosphere Interactions in Radiative-convective Equilibrium Simulations<\/td>\n <\/tr>\n
26<\/td>\n \u90ed\u51a0\u5ef7 <\/td>\n Impact of CRM-GCM Coupling on Tropical Cyclone Simulations using the Superparameterization Framework<\/td>\n <\/tr>\n
27<\/td>\n \u738b\u4fca\u5bd3 <\/td>\n \u6c23\u5019\u8b8a\u9077\u8cc7\u6599\u52a0\u503c\u61c9\u7528\uff1a\u300a\u81fa\u7063\u6c23\u5019\u8b8a\u9077\u95dc\u9375\u6307\u6a19\u5716\u96c6\uff1aAR6\u7d71\u8a08\u964d\u5c3a\u5ea6\u7248\u300b <\/td>\n <\/tr>\n
28<\/td>\n \u6d2a\u6d69\u54f2 <\/td>\n Ozone-Dynamics Feedbacks in an Idealized Model<\/td>\n <\/tr>\n
29<\/td>\n \u9673\u67cf\u8a00 <\/td>\n The characteristic of cold pools over complex topography in TaiwanVVM<\/td>\n <\/tr>\n
30<\/td>\n \u90ed\u73ee\u8431 <\/td>\n \u6c23\u8c61\u5c40\u65b0\u4e00\u4ee3\u5c55\u671f\u5929\u6c23\u9810\u5831\u7cfb\u7d71\u767c\u5c55\u73fe\u6cc1 <\/td>\n <\/tr>\n
31<\/td>\n \u90b5\u5141\u9293 <\/td>\n \u53f0\u7063\u8de8\u5c3a\u5ea6\u6d77\u6c23\u8026\u5408\u6a21\u5f0f\u4e4b\u767c\u5c55 <\/td>\n <\/tr>\n
32<\/td>\n \u738b\u6bd3\u7407 <\/td>\n Novel Perspectives on Diurnal Convection over Complex Topography through VVM Simulations<\/td>\n <\/tr>\n
33<\/td>\n \u9673\u9038\u660c <\/td>\n Leveraging Cloud Resolving Model Data and UNet for Subgrid Cold Pool Intensity Prediction<\/td>\n <\/tr>\n
34<\/td>\n \u9673\u51a0\u6770 <\/td>\n Effect of model resolution on simulation of tropical cyclone landfall in East Asia based on a comparison of 25\u2011 and 50\u2011km HiRAMs<\/td>\n <\/tr>\n
35<\/td>\n \u7f85\u96c5\u862d <\/td>\n The Impact of 3-D Topography effect over Tibetan Plateau on Indian Summer Monsoon: An Assessment from TaiESM<\/td>\n <\/tr>\n
36<\/td>\n \u9ad8\u5bcc\u8056 <\/td>\n An LES Study of Nonlocal Effects of Convective Buoyancy<\/td>\n <\/tr>\n
37<\/td>\n \u6797\u66f8\u6b63 <\/td>\n Assessment of an Experimental Version of fvGFS for TC Genesis Forecasting Ability in the Western North Pacific<\/td>\n <\/tr>\n<\/table><\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
\n\n\n\n\t\t\t\t\n\t\t\t\t\t\t\t\t\t\tNext day\t\t\t\t<\/a>\n\n\t\t\t\t<\/div>\n\n\t\t\t\n\t\t<\/div>\n\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t\t
\n\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\n\t\t
\n\n\t\t\t\n\t\t\t\t
Poster Section II<\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
\n\n\t\t\t\t\t
Day 3 (8\/23) 10:30-12:00<\/div>\n\n\t\t\t\t\t\n\t\t\t\t<\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
\n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n \n
1<\/td>\n \u5f90\u555f\u6853 <\/td>\n Tracking Tropical Low-pressure Systems Related to Equatorial Rossby Waves<\/td>\n <\/tr>\n
2<\/td>\n \u9673\u662d\u5b89 <\/td>\n Impacts of Regional SST Warming on the Western North Pacific Under Global Warming<\/td>\n <\/tr>\n
3<\/td>\n \u9673\u97fb\u5b89 <\/td>\n \u591a\u7a2e\u8056\u5b30\u73fe\u8c61\u5c0d\u6771\u4e9e\u5730\u5340\u6625\u96e8\u7684\u5f71\u97ff\u53ca\u6a5f\u5236\u63a2\u8a0e <\/td>\n <\/tr>\n
4<\/td>\n \u90b1\u51a0\u9298 <\/td>\n \u8056\u5b30\u73fe\u8c61\u5c0d\u53f0\u7063\u6d77\u5cfd\u98a8\u529b\u767c\u96fb\u7cfb\u7d71\u5efa\u7f6e\u4e4b\u98a8\u901f\u8a55\u4f30 <\/td>\n <\/tr>\n
5<\/td>\n \u9ec3\u504c\u6829 <\/td>\n Future Projection and Variability of Kuroshio Under Global Warming<\/td>\n <\/tr>\n
6<\/td>\n \u5f90\u5b50\u6db5 <\/td>\n Using ST Observation to Get the Characteristic of the Boundary Layer Development -the Surface Heat Fluxes and the Entrainment Rate<\/td>\n <\/tr>\n
7<\/td>\n Chia-Wei Lan<\/td>\n Trends in Dry Season Terrestrial Precipitation from 1979 to 2021<\/td>\n <\/tr>\n
8<\/td>\n \u65bd\u749f\u5b8f <\/td>\n Evaluating the Mechanism and Climate Change Impact on the Diurnal Hysteresis between Near Surface Temperature and Relative Humidity<\/td>\n <\/tr>\n
9<\/td>\n \u694a\u5b50\u7469 <\/td>\n The Resilience of Micro-climate in Eastern Taiwan Montane Cloud Forest Areas<\/td>\n <\/tr>\n
10<\/td>\n \u6b50\u5fb7\u6631 <\/td>\n A Novel Approach of Using High Spatiotemporal Geostationary Satellite to Explore the Characteristics of Near-surface Solar Energy Attenuation<\/td>\n <\/tr>\n
11<\/td>\n \u8a31\u54f2\u744b <\/td>\n \u63a2\u8a0e\u5f71\u97ff\u592a\u5e73\u6d0b\u9baa\u985e\u8c50\u5ea6\u540c\u6b65\u8b8a\u52d5\u95dc\u4fc2\u56e0\u5b50\u7279\u6027\u4e4b\u7814\u7a76 <\/td>\n <\/tr>\n
12<\/td>\n \u6797\u80b2\u614e <\/td>\n Influence of Equatorial Pacific Ocean Circulation Bias on El Ni\u00f1o Behavior in CMIP6 simulations<\/td>\n <\/tr>\n
13<\/td>\n \u66fe\u5f18\u6bc5 <\/td>\n Evolution of the Tropical Pacific SST Responses to Extratropical Thermal Forcings<\/td>\n <\/tr>\n
14<\/td>\n \u90ed\u82ae\u4f36 <\/td>\n \u5370\u5ea6\u6d0b\u5076\u6975(IOD)\u548c\u8056\u5b30(ENSO)\u73fe\u8c61\u5c0d\u81fa\u7063\u964d\u96e8\u4e4b\u5f71\u97ff\u5206\u6790 <\/td>\n <\/tr>\n
15<\/td>\n \u7fc1\u6625\u96c4 <\/td>\n Air-Sea Interaction Mechanism of Northward Propagation of Boreal Summer Intraseasonal Oscillation in Tropical Northwestern Pacific<\/td>\n <\/tr>\n
16<\/td>\n \u8521\u776b\u8476 <\/td>\n Pacific Meridional Mode implicated as a prime driver decadal summer temperature variability over Taiwan<\/td>\n <\/tr>\n
17<\/td>\n \u5f35\u8b6f\u5fc3 <\/td>\n The Effect of Forest in Dampening the Diurnal Cycle on Land-atmosphere<\/td>\n <\/tr>\n
18<\/td>\n \u674e\u6b63\u5b89 <\/td>\n Advantages of GSMaP data for Multi-timescale Precipitation Estimation in Luzon<\/td>\n <\/tr>\n
19<\/td>\n \u9ec3\u5a49\u5982 <\/td>\n Characteristics and causes of Taiwan's extreme rainfall in 2022 January and February<\/td>\n <\/tr>\n
20<\/td>\n \u838a\u6137\u6069 <\/td>\n The Impact of Future Long-term Climate Change on the stationary Rainband over Taiwan in the Mei-yu season: The 2 June 2017 Event<\/td>\n <\/tr>\n
21<\/td>\n \u9673\u52c7\u5fd7 <\/td>\n A robust increase in South Asian monsoon rainfall under global warming driven by Southern Ocean heat uptake and Eurasia cloud changes<\/td>\n <\/tr>\n
22<\/td>\n \u5f35\u6def\u7fd4 <\/td>\n The cascade of determining precipitation hotspots of summertime afternoon thunderstorms in northern Taiwan: from synoptic scale to local scale<\/td>\n <\/tr>\n
23<\/td>\n \u674e\u6df3\u5f18 <\/td>\n Exploring Climate Responses to Different Magnitudes of Deforestation in Maritime Continent<\/td>\n <\/tr>\n
24<\/td>\n \u856d\u7acb\u670b <\/td>\n A Revised Tropical Cyclone Genesis Potential Index for Tropical Cyclone Projection in the Western North Pacific<\/td>\n <\/tr>\n
25<\/td>\n \u9ec3\u5b89\u5104 <\/td>\n \u4ee5\u89c0\u6e2c\u8207TaicAM \u6a21\u64ec\u63a2\u8a0e \u6d77\u6eab\u4e0a\u5347\u8da8\u52e2\u5c0d\u6885\u96e8\u6975\u7aef\u964d\u6c34\u7684\u5f71\u97ff <\/td>\n <\/tr>\n
26<\/td>\n \u8449\u82b3\u5229 <\/td>\n \u92d2\u9762\u5075\u6e2c\u7684\u61c9\u7528 <\/td>\n <\/tr>\n
27<\/td>\n \u6797\u601d\u7a4e <\/td>\n Impact of Pacific\u2013Japan pattern on temperature and heatwave events in summer over Taiwan<\/td>\n <\/tr>\n
28<\/td>\n \u8b1d\u65fb\u8015 <\/td>\n A Novel Physics-Informed Neural Network Approach for Downscaling Local Circulation in Taiwan<\/td>\n <\/tr>\n
29<\/td>\n \u85cd\u8a60\u8000 <\/td>\n How much SST feedback periodicity is necessary to maintain robust eastward propagation in coupled model.<\/td>\n <\/tr>\n
30<\/td>\n \u76ae\u5bb6\u5bb9 <\/td>\n Kinetic Treatment in Condensation Process with GTS (Global Forecast System \u2013 Taiwan Earth System Model \u2013 Sundqvist) in Climate Model<\/td>\n <\/tr>\n
31<\/td>\n Mohammed Abdul Athick AS<\/td>\n Breakdown of spatial domain filters for NetCDF and satellite image enhancement.<\/td>\n <\/tr>\n
32<\/td>\n \u66fe\u5c11\u79b9 <\/td>\n Tracking the Rainfall Structure in DYAMOND Convection Permitting Models over the Northwest Pacific<\/td>\n <\/tr>\n
33<\/td>\n \u8303\u7950\u8ed2 <\/td>\n The Effects of Local Circulation and NOx Chemistry on Local Pollutant Transport using Idealized Large Eddy Simulations<\/td>\n <\/tr>\n
34<\/td>\n \u9673\u9d6c\u4efb <\/td>\n Machine Learning Detection of Fog\/Low Cloud over Eastern Taiwan Mountains from Himawari-8 Satellite True-color Image<\/td>\n <\/tr>\n
35<\/td>\n \u90ed\u97cb\u8fb0 <\/td>\n \u521d\u6b65\u63a2\u8a0eTaiESM\u53c3\u6578\u5316\u65b9\u6cd5\u5c0dDouble ITCZ\u6a21\u64ec\u7684\u5f71\u97ff <\/td>\n <\/tr>\n
36<\/td>\n \u5f35\u5de7\u8587 <\/td>\n A Machine Learning Approach to Unraveling the Complex Relationship between Air Pollution and Weather<\/td>\n <\/tr>\n<\/table><\/div>\n\n\t\t\t\n\t\t\t\n\t\t\t\t
\n\n\n\n\t\t\t\t\n\t\t\t\t\t\t\t\t\t\tNext day\t\t\t\t<\/a>\n\n\t\t\t\t<\/div>\n\n\t\t\t\n\t\t<\/div>\n\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t\t
\n\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t\t\t\t
\n\t\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\t\t\t\t8\/21 MON<\/span>\n\t\t\t\t\t<\/span>\n\t\t\t\t\t<\/a>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t\t\t\t
\n\t\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\t\t\t\t8\/22 TUE<\/span>\n\t\t\t\t\t<\/span>\n\t\t\t\t\t<\/a>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t\t\t\t
\n\t\t\t\t\t\n\t\t\t\t\t\t\n\t\t\t\t\t\t\t\t\t8\/23 WEN<\/span>\n\t\t\t\t\t<\/span>\n\t\t\t\t\t<\/a>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
\n\t\t\t\t\t
\n\t\t\t\n\t\n<\/svg>\n\t\t<\/div>\n\t\t\t\t\t
\n\t\t\t\t\t
\n\t\t\t
\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"

Day 2-3 8\/22\u300123 Posters \u5730\u9ede\uff1a\u4e2d\u7814\u9662\u4eba\u6587\u9928\u9928\u5317\u68df3\u6a13\u7b2c\u4e00\u6703\u8b70\u5ba4\u6642\u9593\uff1a2023\/08\/2 […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":476,"menu_order":4,"comment_status":"closed","ping_status":"closed","template":"","meta":{"ocean_post_layout":"full-screen","ocean_both_sidebars_style":"","ocean_both_sidebars_content_width":0,"ocean_both_sidebars_sidebars_width":0,"ocean_sidebar":"0","ocean_second_sidebar":"0","ocean_disable_margins":"on","ocean_add_body_class":"","ocean_shortcode_before_top_bar":"","ocean_shortcode_after_top_bar":"","ocean_shortcode_before_header":"","ocean_shortcode_after_header":"","ocean_has_shortcode":"","ocean_shortcode_after_title":"","ocean_shortcode_before_footer_widgets":"","ocean_shortcode_after_footer_widgets":"","ocean_shortcode_before_footer_bottom":"","ocean_shortcode_after_footer_bottom":"","ocean_display_top_bar":"default","ocean_display_header":"default","ocean_header_style":"","ocean_center_header_left_menu":"0","ocean_custom_header_template":"0","ocean_custom_logo":0,"ocean_custom_retina_logo":0,"ocean_custom_logo_max_width":0,"ocean_custom_logo_tablet_max_width":0,"ocean_custom_logo_mobile_max_width":0,"ocean_custom_logo_max_height":0,"ocean_custom_logo_tablet_max_height":0,"ocean_custom_logo_mobile_max_height":0,"ocean_header_custom_menu":"0","ocean_menu_typo_font_family":"0","ocean_menu_typo_font_subset":"","ocean_menu_typo_font_size":0,"ocean_menu_typo_font_size_tablet":0,"ocean_menu_typo_font_size_mobile":0,"ocean_menu_typo_font_size_unit":"px","ocean_menu_typo_font_weight":"","ocean_menu_typo_font_weight_tablet":"","ocean_menu_typo_font_weight_mobile":"","ocean_menu_typo_transform":"","ocean_menu_typo_transform_tablet":"","ocean_menu_typo_transform_mobile":"","ocean_menu_typo_line_height":0,"ocean_menu_typo_line_height_tablet":0,"ocean_menu_typo_line_height_mobile":0,"ocean_menu_typo_line_height_unit":"","ocean_menu_typo_spacing":0,"ocean_menu_typo_spacing_tablet":0,"ocean_menu_typo_spacing_mobile":0,"ocean_menu_typo_spacing_unit":"","ocean_menu_link_color":"","ocean_menu_link_color_hover":"","ocean_menu_link_color_active":"","ocean_menu_link_background":"","ocean_menu_link_hover_background":"","ocean_menu_link_active_background":"","ocean_menu_social_links_bg":"","ocean_menu_social_hover_links_bg":"","ocean_menu_social_links_color":"","ocean_menu_social_hover_links_color":"","ocean_disable_title":"default","ocean_disable_heading":"default","ocean_post_title":"","ocean_post_subheading":"","ocean_post_title_style":"","ocean_post_title_background_color":"","ocean_post_title_background":0,"ocean_post_title_bg_image_position":"","ocean_post_title_bg_image_attachment":"","ocean_post_title_bg_image_repeat":"","ocean_post_title_bg_image_size":"","ocean_post_title_height":400,"ocean_post_title_bg_overlay":0.5,"ocean_post_title_bg_overlay_color":"","ocean_disable_breadcrumbs":"default","ocean_breadcrumbs_color":"","ocean_breadcrumbs_separator_color":"","ocean_breadcrumbs_links_color":"","ocean_breadcrumbs_links_hover_color":"","ocean_display_footer_widgets":"default","ocean_display_footer_bottom":"default","ocean_custom_footer_template":"0","osh_disable_topbar_sticky":"default","osh_disable_header_sticky":"default","osh_sticky_header_style":"default","osh_sticky_header_effect":"","osh_custom_sticky_logo":0,"osh_custom_retina_sticky_logo":0,"osh_custom_sticky_logo_height":0,"osh_background_color":"","osh_links_color":"","osh_links_hover_color":"","osh_links_active_color":"","osh_links_bg_color":"","osh_links_hover_bg_color":"","osh_links_active_bg_color":"","osh_menu_social_links_color":"","osh_menu_social_hover_links_color":"","slim_seo":{"title":"CHiA Forum 2023 Poster - Climate Hotpots in Action (CHiA) Forum","description":"Day 2-3 8\/22\u300123 Posters \u5730\u9ede\uff1a\u4e2d\u7814\u9662\u4eba\u6587\u9928\u9928\u5317\u68df3\u6a13\u7b2c\u4e00\u6703\u8b70\u5ba4 \u6642\u9593\uff1a2023\/08\/21-2023\/08\/23 8\/21 MON 8\/22 TUE 8\/23 WEN Poster Section I Day 2 (8\/22) 16:00-17:30 1 \u674e\u5b9c\u4ead 2013-2022\u5e74\u677e\u5c71\u6a5f\u5834\u4f4e\u7a7a"},"footnotes":""},"class_list":["post-485","page","type-page","status-publish","hentry","entry"],"_links":{"self":[{"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/pages\/485","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/comments?post=485"}],"version-history":[{"count":0,"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/pages\/485\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/pages\/476"}],"wp:attachment":[{"href":"https:\/\/hydro.as.ntu.edu.tw\/chia\/wp-json\/wp\/v2\/media?parent=485"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}